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First Evidence of Human-Caused Climate Change Melting the West Antarctic Ice Sheet

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An aerial view of Getz ice shelf in West Antarctica taken from a helicopter in January 2018 after using radar on the ice to measure ocean-driven ice shelf melt
Credit: .Pierre Dutrieux

A new study reveals the first evidence of a direct link between human-induced global warming and melting of the West Antarctic Ice Sheet. A research team led by the British Antarctic Survey that included the University of Washington found that curbing greenhouse gas emissions now could reduce this region’s future contribution to global sea level rise.

Ongoing ice loss in West Antarctica has increased over the past few decades. Scientists previously found that ice loss in this region is caused by ocean-driven melt, and that varying winds in the region cause transitions between relatively warm and cool ocean conditions around key glaciers. But until now it was unclear how these naturally occurring variations in the winds could cause ongoing ice loss.

The study by U.S. and U.K. scientists published Aug. 12 in Nature Geoscience finds that in addition to the natural variations, which last about a decade, there has been a longer-term change in the winds that can be linked with human activities. Continued ice loss in this region could cause global oceans to rise tens of inches by the year 2100.

“These results solve a longstanding puzzle,” said co-author Eric Steig, a UW professor of Earth and space sciences. “We have known for some time that varying winds near the West Antarctic Ice Sheet have contributed to the ice loss, but it has not been clear why the ice sheet is changing now.”

“Our work with ice cores drilled in the Antarctic Ice Sheet have shown, for example, that wind conditions have been similar in the past,” Steig said. “But the ice core data also suggest a subtle long-term trend in the winds. This new work corroborates that evidence and, furthermore, explains why that trend has occurred.”

The researchers combined satellite observations and climate model simulations to understand how winds over the ocean near West Antarctica have changed since the 1920s in response to rising greenhouse gas concentrations. They found that human-induced climate change has caused a long-term change in the winds, and that as a result, warm ocean conditions have gradually become more prevalent.

A view of Dotson ice shelf in West Antarctica taken in January 2009 aboard the R/V Nathaniel B. Palmer after deploying an autonomous underwater vehicle under Pine Island ice shelf

Credit: .Pierre Dutrieux

“The impact of human induced climate change on the West Antarctic Ice Sheet is not simple,” said lead author Paul Holland at the British Antarctic Survey. “This is the first evidence for a direct link between human activities and the loss of ice from West Antarctica. Our results imply that a combination of human activity and natural climate variations have caused ice loss in this region, accounting for around 4.5 centimeters [1.8 inches] of sea level rise per century.”

Previous research from Steig and co-author Pierre Dutrieux, a research assistant professor at Columbia University and former UW research scientist, had established the connection between the ocean currents, winds and the West Antarctic Ice Sheet.

“We knew this region was affected by natural climate cycles lasting about a decade, but these didn’t necessarily explain the ice loss,” Dutrieux said. “Now we have evidence that a century-long change underlies these cycles, and that it is caused by human activities.”

The team also looked at model simulations of future winds, and found that if greenhouse gas emissions continue to rise, the winds will continue to shift in a way that increases the rate of ice loss. But if greenhouse gas emissions are controlled, the winds remain in their current state and prevent greater warming to the underside of the ice sheet.

Other co-authors are Thomas Bracegirdle and Adrian Jenkins at the British Antarctic Survey. The research was funded by the U.S. National Science Foundation.

Contacts and sources:
University of Washington
British Antarctic Survey (BAS)

Citation:West Antarctic ice loss influenced by anthropogenic forcing and internal climate variability is published by Paul R. Holland, Thomas J. Bracegirdle, Pierre Dutrieux, Adrian Jenkins and Eric J. Steig in the journal Nature Geoscience. Read it here: https://www.nature.com/articles/s41561-019-0420-9


Source: http://www.ineffableisland.com/2019/08/first-evidence-of-human-caused-climate.html


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    Total 3 comments
    • raburgeson

      They have no such evidence. Explain the increased temperatures in the rest of the solar system.

    • wheeties

      your article is total nonsense,bullshett-man has zero impact on weather,zero– one volcano puts as much pollution in a month as man does world wide does in a year–there is over 40 active volcanoes right now–plus the sun—-> we are in solar minimums right now–the sun by thousands of times has bigger impact over weather than all the farts coming out of carbon use–during very high carbon emissions by volcanoes millions of years ago the plant life went nuts–the jungles were huge–plant life loves carbon,its food —but your an moron,idiot so its a waste of time to talk to retards that have a polictical agenda,ie,get rid of cars–your a fool

    • DK

      The paper starts its core samples from the 1920′s its behind a paywall but one of the authors makes the claim: The Antarctic ice sheet is melting and, yeah, it’s probably our fault. Filed under: Climate Science — eric @ 14 August 2019(http://www.realclimate.org/) Erik Steig

      “In short, glacier melt in West Antarctica has increased because more Circumpolar Deep Water (which is relatively warm) is getting from the ocean surrounding Antarctica onto the Antarctic continental shelf and reaching the floating ice shelves of the large outlet glaciers that drain the West Antarctic ice sheet into the ocean. As shown by Thoma et al. (2008) in a seminal modeling study in Geophysical Research Letters**, how much Circumpolar Deep Water (CDW) gets onto the continental shelf is strongly influenced by the strength and direction of the winds at the shelf edge. Essentially, stronger westerlies (or simply weaker easterlies) tend to cause more CDW inflow, and hence, more glacial melt.

      Because of the important role played by the winds, many have assumed that there must be a link between the melting glaciers and the ozone hole. But the greatest control on wind variability along the coast of West Antarctica is the state of the tropics. Just as El Niño event causes widespread climate anomalies in the Northern Hemisphere — such as increased rainfall in southern California — it also causes changes in the West Antarctic. Indeed, the Amundsen Sea, where the largest West Antarctic glaciers are, is one of the areas on the planet that is most strongly dependent on the El Niño-Southern Oscillation (ENSO) (e.g. Lachlan-Cope and Connolley, 2006). In 2012, we published a paper showing that changes in the winds in this region in the last few decades, which correspond well with variations in the glaciers, are very well explained by changes in ENSO, and very poorly by changes in ozone. We also noted that because big ENSO events had occurred in the past, it was quite plausible that wind conditions not that different than those of today had also occurred in the past. Indeed, we have very good evidence from ice cores that climate conditions in West Antarctica in the 1940s were not very different than those in the 1990s.

      It is clear from this work, and much other recent research, that ENSO plays a dominant role in determining the climate conditions in West Antarctica that are relevant to the ice sheet. And since there is little evidence for a long-term anthropogenic change in ENSO, this implies that natural variability in Amundsen Sea winds (driven by natural variability in ENSO) may be the primary driver of observed ice-sheet change in West Antarctica in the last few decades. This is what Richard Alley is referring when he says that the evidence for forcing by natural variability was strong, and it throws a lot of cold water (no pun intended) on the purported link with human activities. But that’s not very satisfying. It doesn’t answer the question of why glacier retreat is occuring now. This is where our new paper comes in.

      The new work is led by Paul Holland of the British Antarctic Survey (BAS), with help from Tom Bracegirdle, Adrian Jenkins (also of BAS), Pierre Dutrieux (now at LDEO) and myself. What we argue, in brief, is that although ENSO does indeed dominate the wind variability in the Amundsen Sea on timescales from interannual to multi-decadal, there is also a longer-term trend in the winds, on which the ENSO-related variability is superimposed.

      The graph below (Figure 1) summarizes the key finding. What is shown are the winds in the key sector of the Amundsen Sea, centered on ~71°S and ~108°W, with observations in blue, and model results in black and gray. The model results are from an ensemble of simulations, referred to as the “tropical pacemaker” or “PACE” runs, of the CESM climate model. Details are given in Schneider and Deser (2017). Briefly, what has been done is to adjust an otherwise free-running climate model (forced by greenhouse gas emissions) so that it follows the actual history of sea surface temperature in the tropics, but is otherwise left unconstrained by data. We use these experiments as an estimate of how winds have varied over the last century in the Amundsen Sea, a) given what we know happened in the tropics and b) given what the climate model’s physics dictates about how conditions in the tropics affect the Amundsen Sea. Critically, there is nothing done to make the model match observations outside the tropics. Yet the results are in superb agreement with the observed Amundsen Sea winds. While we can never know exactly what happened prior to the advent of satellite observations in the late 1970s, the PACE ensemble provides a set of histories that is plausible, and compatible with modern data. This is probably the best current estimate of how winds have in fact varied in this region.”

      In other words they are using a current climate model one of 800 or so which happens to correlate with their observations on ice loss, because the model shows in a graph forcing over 10 year cycles to 1920 then it must be greenhouse gases therefore human induced climate change, there is a little secret I must pass on, the deep sea ocean currents are 500 & 800 year cycles where CO2 at 50x atmospheric levels gets stored in a long term sink and released in later centuries, Climate models have never modelled the ocean, CO2 has absolutely no effect on sea temperature ABSOLUTELY NONE. :lol: So to get their conclusion, they ignore 120,000 years of prior atmospheric sampling and temperature data to ignore the entire world pe 1920′s that the ENSO which they blame for winds is entirely solar activity driven, CO2 levels at the present are from the medieval warming period, if you in fact ignore everything but what they include in the paper,it is confirmation bias science. :lol:

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